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How does nitrogen get from our homes into Waquoit Bay, and what does it do there? The 1992 study that connected land and bay

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The short version

In the early 1990s, a team of twelve scientists led by Ivan Valiela set out to show how what happens on land shapes Waquoit Bay. They compared parts of the bay whose watersheds ranged from mostly forest to heavily built up with homes on septic systems. Where there was more development, groundwater reaching the shore carried much more nitrogen, and the water showed it: more algae, more seaweed, more frequent oxygen crashes, less eelgrass and different bottom life. The paper laid out the chain from septic system to seaweed that later research, and today’s cleanup plans, build on.

What the researchers did

The study used Waquoit Bay’s sub-watersheds as a natural experiment. (The full article is behind a paywall; this summary is based on its published abstract.)

  • They chose sub-watersheds that differ in how developed they are, measured by the number of septic systems and the amount of forest, so that each part of the bay receives a very different nutrient load.
  • They followed groundwater, the main way nutrients travel from land to the bay in this area, and measured what it carried as it reached the shore.
  • In the receiving waters they tracked nutrients, floating algae (phytoplankton), seaweed, eelgrass, oxygen and the animals living on the bottom.

What they found

  • Groundwater is the delivery route. Nitrogen from the watershed reaches the bay mainly by seeping in through groundwater rather than running off the surface.
  • Some nitrogen is lost on the way, but not enough. Part of it is removed in the aquifer or where groundwater passes through the bay’s bottom sediments. Even so, in built-up areas groundwater arrived at the shore with significantly more nutrients, enough to change the bay.
  • More nitrogen, more algae. Where loading was higher, the water held more nutrients, phytoplankton grew faster, and seaweed grew faster and piled up.
  • Seaweed takes over. Thick seaweed came to dominate, changing the water’s nutrient balance and making oxygen-free (anoxic) events more frequent. As seaweed spread, the area covered by eelgrass shrank.
  • Bottom life changes too. The switch from eelgrass to seaweed, together with more frequent low oxygen, changed which animals live on the bay floor.
  • Not a simple formula. Because so many steps lie between a house and the bay, the authors warned against expecting a one-to-one match between land use and water quality, and called for models to make sense of the chain.

What it means for Waquoit Bay today

This is one of the founding papers of Waquoit Bay science. Its central message, that the bay’s health is controlled from the bottom of the food web by how much nitrogen arrives from the land, is the basis for the nitrogen limits that Falmouth and Mashpee now plan around. The team’s later work turned this picture into estimates of where the nitrogen comes from (see where Waquoit Bay’s nitrogen comes from) and traced septic nitrogen into the bay’s plants (see the chemical fingerprint study).

This summary is based on the abstract.

Read the paper

Valiela, I., Foreman, K., LaMontagne, M., Hersh, D., Costa, J., Peckol, P., DeMeo-Andreson, B., D’Avanzo, C., Babione, M., Sham, C.-H., Brawley, J., & Lajtha, K. (1992). Couplings of watersheds and coastal waters: Sources and consequences of nutrient enrichment in Waquoit Bay, Massachusetts. Estuaries, 15(4), 443–457. https://doi.org/10.2307/1352389

License: © 1992 Estuarine Research Federation, published by Springer. The article is not openly licensed and the full text is behind a paywall, so we link to the publisher’s page rather than host a copy; this summary is based on the published abstract. The card image is a title card made from the citation.

Drafted with AI assistance from the linked source.